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The Gauja Formation is a Middle Devonian fossil locality in Estonia and Latvia.〔(【引用サイトリンク】title=Gauja Stage )〕 It is named after the Gauja River, where it is exposed along the banks.〔(【引用サイトリンク】title=Gauja River )〕 The Gauja Formation has a maximum thickness of . It is composed of weakly to moderately cemented layers of fine-grained to very fine-grained sandstone. The layer is predominantly light to yellowish-gray in color, but can be pinkish brown or variegated. It is mostly composed of quartzose arenites. It is overlain by the thick Amata Formation and the Plavinas Formation. The Gauja Formation contains two cyclic members. The lower layers are known as the Sietin Member and are composed mostly of sandstone with a thin layer of siltstone at the top.〔 It has yielded numerous fossils of fishes. Among them are ''Asterolepis'', ''Bothriolepis'', ''Glyptolepis baltica'', ''Laccognathus panderi'', and ''Megadonichthys kurikae''.〔 The upper layers are thicker, and the lower part of it is known as the Lode Member. The Lode Member dates from the Middle Devonian and is composed of light colored sandstone. The area is indicative of a near-shore environment of retreating sea.〔 Only large plant remains and miospores are known from this member. Examples of which include ''Hostinella'', ''Archaeopteris'', ''Retusotriletes rugulatus'', and ''Ancyrospora''. Palynological studies indicate that the Middle to Upper Devonian boundary may exist in this member. ==See also== *List of fossil sites *Gauja National Park *Gauja valley 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「Gauja Formation」の詳細全文を読む スポンサード リンク
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